Biodiversity
 

 

Amsterdam Water Supply Dunes
 
Natural Values and Functions
Geology and Genesis
Management
Drinking Water Supply
Nature Management
Tourism and Recreation

 

 

 

 

 

 

 

 

 
Coastal Guide on Dune Management 
 
The Amsterdam Water Supply Dunes (The Netherlands)


Drinking Water Supply

History
In 1951 the Municipality of Amsterdam bought the first dune areas for the purpose of producing drinking water, followed by other pieces of dune area during the 19th century. The first supply of dune water dates from 1853, to the people of Amsterdam. Because of the abstraction of the water the dune area became more and more desiccated, with negative effects on flora, fauna and landscape. In 1957 river water (from the Rhine) was infiltrated in the Amsterdam Water Supply Dunes to overcome the desiccation and use the dunes to naturally filter the river water to produce drinking water. This however, had another big negative effect on nature: eutrophication. The artificial input of river water caused damage to the ecological quality of dune lakes and adjacent slacks as a result of a massive increase in nutrients. Also, large areas were excavated to transport the river water into the dunes. Therefore, since 1973 the river water is piped from the River Rhine and infiltrated after intensive pre-purification. In this day, 70 million m3 of drinking water is extracted from the Amsterdam Water Supply Dunes, supplying approximately 1,1 million users in the city of Amsterdam and its surroundings.

Method
The water that is infiltrated in the Amsterdam Water Supply Dunes is rainwater and water from the River Rhine, which is taken in from the Lek canal at Nieuwegein. Along the River Rhine several measuring stations are located, from Switzerland to the Netherlands. These stations check the quality of the water. In case hazardous substances are found, the intake of water stops immediately.
The water is pre-purificated before it is transported to the dunes. The water is transported through 3 pipelines with a total length of 210 kilometres into two small lakes at the east side of the Amsterdam Water Supply dunes. From there, it streams into infiltration canals, which are 35 metres wide and several kilometres long. The water slowly infiltrates into the ground and raises the groundwater level. The groundwater storage is enough to provide the city of Amsterdam 2 months of drinking water. The water has a residence time between 60 and 400 days and in this period natural, biological processes purify the water.

Through drains the water is collected from the dunes into a canal, from which the water streams to the Oranjekom (a small lake) under natural fall. From the Oranjekom the water is pumped to the purification plants. Here the water is further purificated to be used as drinking water.
The drinking water is stored into two double storage tanks from where it is distributed according to the need of the users. The total net of water pipes is about 2000 kilometres long.

Water supply and nature management
Water abstraction and nature conservation are the two primary functions of the Amsterdam Water Supply Dunes. Previous research and future research is aimed at finding an optimum between water abstraction and nature. It is not an option to stop the drinking water production completely in favour of nature management. This, because the dunes provide a safe storage and supply of water of the highest quality.

Since 1989 an extensive multi-disciplinary research started in combining water supply and nature management and in 1998 an eco-hydrological survey was completed. Several projects have already been implemented (see: Nature management).

There is also research being done about other ways to infiltrate the water, for example deep-well-infiltration. This would allow the infiltration canals to (partly) disappear and restoring the original geomorphology in this part of the dunes. Benefits of deep-well-infiltration are that the groundwater supply in the deeper underground becomes larger and the chance of desiccation of the current infiltration area at the surface becomes smaller. Problems with deep-well-infiltration are the high cost and the fact that the location of the deep-infiltration should be in the dunes, because of the protection of the groundwater and the limited size of the freshwater body beneath the dunes.

Result
Water abstraction provides a financially solid base for nature conservation.
Nature conservation is an effective protection for water resources and makes it possible to gain public support and trust.
 

References:

  • Amsterdam Water Supply Dunes (1998) Amsterdam Water Supply Dunes; Implementation of eco-hydrological research; in: Coastline 7-3, EUCC. (KJd)
  • Beekelaar W.K.A.G. & Geelen L.H.W.T. (1999) Management scheme 2000-2010; new challenges in the Amsterdam Watersupply Dunes; in: (ed) Rabski K.: Connecting science and management in the coastal zone; proceedings of the 7th EUCC International conference Coastlines ’99, held in Miedzyzdroje, Poland, june 7-12 1999. (PC1999e#)
  • Janssen M. (1993) Natuur in ontwikkeling; in: Duin: Themanummer Amsterdamse Waterleidingduinen, no.1993-4, Stichting Duinbehoud. (33BCD1993)

 

 




 

 
 
Dune Guide ordered by


Each case can be found via geographical maps and via thematical texts putting the cases in an order of six interesting topics:
seashore dynamics
sand mobility
hydrology and water management
conservation management
management of forests
management in relation to recreation and tourism

 

 

 

Prepared by Laura van Schagen at EUCC International Secretariat